Decoding the Ocean’s Influence on Global Surface Air Temperature Patterns - Part 2
When heat is added to the climate system, it can be challenging to determine where and by how much the surface air temperature will increase. Scientists at the U.S. Department of Energy’s Pacific Northwest National Laboratory led a two-part study that approached this challenge from a unique experimental angle. They constructed the linear response function of surface air temperature intrinsic to Earth’s climate system and the associated temperature patterns under random perturbation—called neutral modes. As a result, the research team confirmed that the global mean surface air temperature is far more responsive to ocean heating from high latitudes than from the tropics.
This work sheds an important new light on recurrent patterns of global surface air temperatures, such as polar amplification, in which warming is greater at the poles than the global mean warming. It also points to a promising direction for predicting regional climate responses to perturbations of Earth’s energy balance.
In a two-part study, researchers performed a large set of model simulations in which they added ocean heat flux patches one patch at a time to cover the global oceans. These so-called Green’s function experiments mimicked the effects of heat absorbed by the ocean. Through the experiments, scientists examined how the global surface air temperature (SAT) responds to random energy perturbations and how atmospheric energy transport compensates for the ocean’s influence, or forcing, at different locations. With the total of 106 pairs of numerical experiments, researchers constructed the linear response function of the SAT to ocean heat fluxes—or any forcing to the atmosphere, for that matter. An analysis of the linear response function revealed the SAT patterns—the neutral modes—that were most excitable due to oceanic forcing. In particular, the first and most dominant neutral mode bore a great resemblance to the pattern of the Interdecadal Pacific Oscillation, a pattern of natural variability at decadal time scales across the Pacific Ocean. Because ocean dynamics were absent from the Green’s function experiments with prescribed ocean heat fluxes, the result implies that the Interdecadal Pacific Oscillation originates from atmospheric processes.
The experiments also confirmed a result from a previous study—derived from more idealized model configuration—that the global mean SAT is far more responsive to ocean heating from high latitudes than from the tropics. This result stemmed from how cloud, ice albedo (reflectivity), water vapor, and atmospheric temperature profiles responded to ocean heating and influenced the SAT. Meanwhile, the tropics showed more “altruism” in sharing the warming with higher latitudes than the other way around. This was likely due to the high energy transport efficiency of the Hadley overturning circulation in the tropics. Remarkably, regardless of the location of the oceanic forcing, the neutral mode of the SAT response gave rise to recurrent features of climate response, the most prominent being the polar-amplified warming.